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How Much Has the Atmospheric Temperature Really Changed?PowerPoint Presentation

How Much Has the Atmospheric Temperature Really Changed?

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How Much Has the Atmospheric Temperature Really Changed?

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How Much Has the Atmospheric Temperature Really Changed?

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How Much Has the Atmospheric Temperature Really Changed?

An Attempt to Resolve the Satellite Dataset Controversy.

John Lanzante (GFDL)

Carl Mears (RSS)

- Evaluate differences between temperatures from 2 leading
- satellite datasets using radiosonde (weather balloon) data
- WORK IN PROGRESS – RESULTS ARE PRELIMINARY!
- RESULTS ARE NOT FROM LATEST VERSIONS OF MSU

SATELLITE DATA USED

- Try to resolve trend differences between 2 satellite datasets
- UAH (Univ. Alabama/Huntsville) Christy & Spencer
- RSS (Remote Sensing Systems) Mears & Wentz
- Time period
- 1979-May 2005 (updating to present with more recent versions)
- Satellite data begins in 1979
- Area averages
- Globe and Tropics (big picture)

SATELLITE DATA: MSU

- Three layers relevant to climate
- Channel 4 (T4) Lower stratosphere
- Channel 2 (T2) Mid/upper troposphere (some stratosphere)
- Artificial channel (TLT) Lower troposphere[no results yet!]

RADIOSONDE DATA USED

- LKS/RATPAC (global 85 station network)
- LKS= Lanzante/Klein/Seidel
- RATPAC = Radiosonde Atmospheric Temperature
- Products for Assessing Climate
- Direct satellite/radiosonde comparisons only at these stations
- Convert to layer averages using appropriate weighting functions

METHODOLOGY: OVERVIEW

Purpose:

Narrow the range of possibilities of “real climate” by critically comparing two satellite temperature datasets (UAH & RSS) that have been adjusted for homogeneity.

Means:

Use a third dataset (RATPAC radiosonde data), that is also subject to concerns about inhomogeneity, in a novel way to “choose” (between UAH & RSS).

Caveat:

Since all 3 datasets have concerns regarding homogeneity, we can’t simply compare long-term trends, satellite vs radiosonde, (as others have done) to decide which satellite dataset is better!

METHODOLOGY: PROCEDURE

- Reduce the dimensionality of the problem
- Use global difference series (RSS-UAH) to identify “events”
- Chose these events in conjunction with satellite metadata
- Events are of 2 types:
- Step: Discrete transition (change in satellite or data use)
- Drift: Gradual change (satellite drift inhomogeneity)
- Note: A few events explain most of (RSS-UAH) trend difference

METHODOLOGY: T4 EVENTS

METHODOLOGY: T2 EVENTS

METHODOLOGY: PROCEDURE

- Compute step or drift metrics for pairs of differences
- (RSS-UAH, RSS-RATPAC & UAH-RATPAC) at radiosonde stations
- Step Difference in means; Drift Linear slope; Both t-test
- Compute summary statistics from station statistics
- For each event declare a “winner” (RSS or UAH) closest to sonde
- Vary the length of the step/drift segments to insure robustness
- Diagnose the events
- Examine maps of station statistics
- Suggest nature of satellite problems?
- Look for radiosonde inhomogeneities (using metadata)
- Adjust the satellite data to ameliorate inhomogeneities
- Adjust using “winner takes all” strategy, event by event
- (adjust “loser” to match “winner”)
- Vary adjustment stringency criterion to create different sets
- Compute trends from various adjustment sets
- Compare trends from different sets with original data

METHODOLOGY: STRENGTHS & WEAKNESSES

- Strength: Minimizes influence of sonde inhomogeneities/biases
- Use global network (not all stations change at same time)
- Examine sonde metadata & maps (look for inhomogeneities)
- Short segments minimize effect of sonde spurious cooling
- No direct adjustment of satellite data by sonde data
- Weakness: “Winner takes all” adjustment strategy
- “Correct” could be intermediate (between RSS & UAH)
- “Correct” could be outside of both (RSS & UAH both wrong)
- Strength: Sensitivity analyses
- Use of different segment lengths tests robustness
- Use of different adjustment criteria tests robustness
- Caveats:
- Any unmitigated sonde biases would likely impart a
- cool bias to the results (our strategy should minimize this)
- We assume no problems outside of “events”

RESULTS: T4 WINNERS

RESULTS: T2 WINNERS

RESULTS: LINEAR TRENDS (T4)

Linear Trends1: Jan1979–May2005 [ (K/decade) X 100) ]

1 Based on median of pair-wise slopes (mps) nonparametric regression

NOTE: Radiosonde trends ~ -65

RESULTS: LINEAR TRENDS (T2)

Linear Trends1: Jan1979–May2005 [ (K/decade) X 100) ]

1 Based on median of pair-wise slopes (mps) nonparametric regression

NOTE: Radiosonde trends ~ 0-2

* THE END *

Supplementary

Slides Follow

Chapter 3, Fig. 1 [CCSP SAP1.1]

Figure 3.1 - Time series of globally averaged surface temperature (TS) for NOAA (violet), NASA (black), and HadCRUT2v (green) datasets. All time series are 7-month running averages (used as a smoother) of original monthly data, which were expressed as a departure (ºC) from the 1979-97 average.

Chapter 3, Fig. 2 [CCSP SAP1.1]

Figure 3.2a - Bottom: Time series of globally averaged tropospheric temperature (T(850-300)) for RATPAC (violet) and HadAT2 (green) radiosonde datasets. All time series are 7-month running averages (used as a smoother) of original monthly data, which were expressed as a departure (ºC) from the 1979-97 average.

Figure 3.2b - Top: Time series of globally averaged stratospheric temperature (T(100-50)) for RATPAC (violet) and HadAT2 (green) radiosonde datasets. All time series are 7-month running averages (used as a smoother) of original monthly data, which were expressed as a departure (ºC) from the 1979-97 average.

Chapter 3, Fig.3 [CCSP SAP1.1]

Figure 3.3a- Bottom: Time series of globally averaged lower tropospheric temperature (T2LT) as follows: UAH (blue) and RSS (red) satellite datasets, and HadAT2 (green) radiosonde data. All time series are 7-month running averages (used as a smoother) of original monthly data, which were expressed as a departure (ºC) from the 1979-97 average.

Figure 3.3b- Third: Time series of globally averaged middle tropospheric temperature (T*G) as follows: UAH (blue) and RSS (red) satellite datasets, and HadAT2 (green) radiosonde data. All time series are 7-month running averages (used as a smoother) of original monthly data, which were expressed as a departure (ºC) from the 1979-97 average.

Figure 3.3c - Second: Time series of globally averaged upper middle tropospheric temperature (T2) as follows: UAH) (blue), RSS (red), and UMd (black) satellite datasets, and HadAT2 (green) radiosonde data. All time series are 7-month running averages (used as a smoother) of original monthly data, which were expressed as a departure (ºC) from the 1979-97 average.

Figure 3.3d - Top: Time series of globally averaged lower stratospheric temperature (T4) as follows: UAH (blue) and RSS (red) satellite datasets, and HadAT2 (green) radiosonde data. All time series are 7-month running averages (used as a smoother) of original monthly data, which were expressed as a departure (ºC) from the 1979-97 average.

Chapter 3, Table 2 [CCSP SAP1.1]

Table 3.2 - Global temperature trends in ºC per decade from 1958 through 2004 (except for ERA40 which terminates September 2001) calculated for the surface or atmospheric layers by data source. The trend is shown for each, with the approximate 95% confidence interval (2 sigma) below in parentheses. The levels/layers, from left to right, go from the lowest to the highest in the atmosphere. Bold values are estimated to be statistically significantly different from zero (at the 5% level). A Student’s t-test, using the lag-1 autocorrelation to account for the non-independence of residual values about the trend line, was used to assess significance (see Appendix A for discussion of confidence intervals and significance testing).

Chapter 3, Table 3 [CCSP SAP1.1]

Table 3.3 - Global temperature trends in ºC per decade from 1979 through 2004 (except for ERA40 which terminates September 2001) calculated for the surface or atmospheric layers by data source. The trend is shown for each, with the approximate 95% confidence interval (2 sigma) below in parentheses. The levels/layers, from left to right, go from the lowest to the highest in the atmosphere. Bold values are estimated to be statistically significantly different from zero (at the 5% level). A Student’s t-test, using the lag-1 autocorrelation to account for the non-independence of residual values about the trend line, was used to assess significance (see Appendix A for discussion of confidence intervals and significance testing).

Chapter 3, Table 4 [CCSP SAP1.1]

Table 3.4 – Tropical (20ºN-20ºS) temperature trends in ºC per decade from 1979 through 2004 (except for ERA40 which terminates September 2001) calculated for the surface or atmospheric layers by data source. The trend is shown for each, with the approximate 95% confidence interval (2 sigma) below in parentheses. The levels/layers, from left to right, go from the lowest to the highest in the atmosphere. Bold values are estimated to be statistically significantly different from zero (at the 5% level). A Student’s t-test, using the lag-1 autocorrelation to account for the non-independence of residual values about the trend line, was used to assess significance (see Appendix A for discussion of confidence intervals and significance testing).

RESULTS: ADJUSTED TIME SERIES (T4)

RESULTS: ADJUSTED TIME SERIES (T2)

TRENDS FROM SHERWOOD & MEYERS (2008)